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The Teschenite Sill of Charlestown, Fife

Published online by Cambridge University Press:  01 May 2009

Frederick Walker
Frederick Walker
Affiliation:
University of St. Andrews
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Extract

Almost all the more important teschenitic intrusions of the Edinburgh district have been examined in some detail at one time or another, but the large sill situated between Dunfermline and Charlestown is a notable exception. In the course of an investigation last autumn, the writer found, however, that, while the normal rock is not specially noteworthy, its segregations present some interesting features, particularly in view of a recent publication by Dr. G. W. Tyrrell dealing with the age and classification of the analcitic intrusions of Central Scotland.

Type
Original Articles
Information
Geological Magazine , Volume 63 , Issue 8 , August 1926 , pp. 343 - 347
Copyright
Copyright © Cambridge University Press 1926

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References

page 344 note 1 Geol. Mag., Vol. LX, 1923, pp. 249–60.Google Scholar

page 344 note 2 Geology of the Edinburgh District, 1910, p. 293.Google Scholar

page 344 note 3 Trans. Roy. Soc. Edin., vol. liii, part 2, p. 372.Google Scholar

page 345 note 1 Geol. Mag., Vol. LIX, 1922, p. 450.Google Scholar

page 346 note 1 Loc. cit.Google Scholar

page 346 note 2 Geol. Mag., Vol. LX, 1923, pp. 530–42.Google Scholar

page 346 note 3 Loc. cit., pp. 250, 251.Google Scholar

page 346 note 4 Geol. Mag., 1912, p. 71.Google Scholar

page 347 note 1 Compare Edinburgh Memoir, pl. xi, fig. 4, with Geol. Mag., 1923, Pl. XI, Fig. 4.Google Scholar

page 347 note 2 Mem. Geol. Surv. Scotland, Glasgow District, 1911, p. 113.Google Scholar